Évolution plutonique et structurale de la presqu'île d'Akuliaruseq, Groenland méridional

Authors

  • F Persoz

DOI:

https://doi.org/10.34194/bullggu.v72.6610

Abstract

The Akuliaruseq area, situated between Julianehåb and Nanortalik, is formed of granites (ca. 75 % of the area) and gneisses belonging to the Canadian-Greenlandic shield. The geological history is divided into five periods of varying significance.

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Published

1969-02-26

Issue

Vol. 72 (1969): Évolution plutonique et structurale de la presqu'île d'Akuliaruseq, Groenland méridional

Section

Monograph

License

This article is distributed under a CC-BY 4.0 licence, permitting free redistribution and reproduction for any purpose, even commercial, provided proper citation of the original work. Author(s) retain copyright over the article contents.

How to Cite

Évolution plutonique et structurale de la presqu’île d’Akuliaruseq, Groenland méridional. (1969). Bulletin Grønlands Geologiske Undersøgelse, 72, 1-202. https://doi.org/10.34194/bullggu.v72.6610